Mysterious deep-Earth seismic signature explained

Mysterious deep-Earth seismic signature explained
The movement of seismic waves through the material of the mantle allows scientists to image Earth's interior, just as a medical ultrasound allows technicians to look inside a blood vessel. Image is courtesy of Edward Garnero and Allen McNamara's 2008 Science paper Structure and Dynamics of Earth's Lower Mantle, provided with Garnero's permission. Credit: Edward Garnero and Allen McNamara

New research on oxygen and iron chemistry under the extreme conditions found deep inside the Earth could explain a longstanding seismic mystery called ultralow velocity zones. Published in Nature, the findings could have far-reaching implications on our understanding of Earth's geologic history, including life-altering events such as the Great Oxygenation Event, which occurred 2.4 billion years ago.

Sitting at the boundary between the lower mantle and the core, 1,800 miles beneath Earth's surface, ultralow velocity zones (UVZ) are known to scientists because of their unusual seismic signatures. Although this region is far too deep for researchers to ever observe directly, instruments that can measure the propagation of seismic waves caused by earthquakes allow them to visualize changes in Earth's interior structure; similar to how ultrasound measurements let medical professionals look inside of our bodies.

These seismic measurements enabled scientists to visualize these ultralow velocity zones in some regions along the core-mantle boundary, by observing the slowing down of seismic waves passing through them. But knowing UVZs exist didn't explain what caused them.

However, recent findings about iron and chemistry under deep-Earth conditions provide an answer to this longstanding mystery.

It turns out that water contained in some minerals that get pulled down into the Earth due to plate tectonic activity could, under extreme pressures and temperatures, split up—liberating hydrogen and enabling the residual oxygen to combine with iron metal from the core to create a novel high-pressure mineral, iron peroxide.

Led by Carnegie's Ho-kwang "Dave" Mao, the research team believes that as much as 300 million tons of water could be carried down into Earth's interior every year and generate deep, massive reservoirs of iron dioxide, which could be the source of the ultralow velocity zones that slow down seismic waves at the .

To test this idea, the team used sophisticated tools at Argonne National Laboratory to examine the propagation of seismic waves through samples of iron peroxide that were created under deep-Earth-mimicking pressure and temperature conditions employing a laser-heated diamond anvil cell. They found that a mixture of normal mantle rock with 40 to 50 percent iron peroxide had the same seismic signature as the enigmatic ultralow velocity zones.

For the research team, one of the most-exciting aspects of this finding is the potential of a reservoir of oxygen deep in the planet's interior, which if periodically released to the Earth's surface could significantly alter the Earth's early atmosphere, potentially explaining the dramatic increase in atmospheric oxygen that occurred about 2.4 billion years ago according to the geologic record.

"Finding the existence of a giant internal oxygen reservoir has many far-reaching implications," Mao explained. "Now we should reconsider the consequences of sporadic oxygen outbursts and their correlations to other major events in the Earth's history, such as the banded- formation, snowball Earth, mass extinctions, flood basalts, and supercontinent rifts."


Explore further

When water met iron deep inside the Earth, did it create conditions for life?

More information: Hydrogen-bearing iron peroxide and the origin of ultralow-velocity zones, Nature (2017). nature.com/articles/doi:10.1038/nature24461
Journal information: Nature

Citation: Mysterious deep-Earth seismic signature explained (2017, November 22) retrieved 24 August 2019 from https://phys.org/news/2017-11-mysterious-deep-earth-seismic-signature.html
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Nov 23, 2017
The existence of such huge geological sources of oxygen in the primordial earth leads to the question of how common such phenomenon are when other planets form.

Nov 24, 2017


This also begs the question:

Based pon what empirical evidence?

Laboratory results don't --in this particular case-- necessarily equate to actual circumstances

There is no known physical process --including plate tectonics-- that can account for the presence of this H2O at this depth, given the chemical properties of any mineral species at this depth/pressure/temperature.

This conclusion rests upon the ability of some hypothetical surface mineralogical species being transported to a depth for which there is no known geophysical/chemical mechanism.

A supposition --IOW-- presumed to be fact.


Nov 24, 2017
What I mean by this is that any water or even hydrated minerals would have given up their H2O --due to prevailing pressure and temperature-- long before they could have been transported via subduction to this depth beneath the Earth's surface.

By standard geochemical processes, at any rate, this makes no sense at all.

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